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READING PASSAGE 4
THE LITTLE ICE AGE
A
This book will provide a detailed examination of the Little Ice Age and other climatic shifts, but, before
I embark on that, let me provide a historical context. We tend to think of climate - as opposed to weather - as
something unchanging, yet humanity has been at the mercy of climate change for its entire existence, with at
least eight glacial episodes in the past 730,000 years. Our ancestors adapted to the universal but irregular
global warming since the
end of the last great Ice Age, around 10,000 years ago, with dazzling opportunism.
They developed strategies for surviving harsh drought cycles, decades of heavy rainfall or unaccustomed cold;
adopted agriculture and stock-raising, which revolutionised human life; and founded the world’s first pre-
industrial civilisations in Egypt, Mesopotamia and the Americas. But the price of sudden climate change, in
famine, disease and suffering, was often high.
B
The Little Ice Age lasted from roughly 1300 until the middle of the nineteenth century. Only two centuries
ago, Europe experienced a cycle of bitterly cold winters; mountain glaciers in the
Swiss Alps were the lowest
in recorded memory, and pack ice surrounded Iceland for much of the year. The climatic events of the Little
Ice Age did more than help shape the modern world. They are the deeply important context for the
current unprecedented global warming. The Little Ice Age was far from a deep freeze, however; rather an
irregular seesaw of rapid climatic shifts, few lasting more than a quarter-century, driven by complex and still
little understood interactions between the atmosphere and the ocean. The seesaw brought cycles of intensely
cold winters and easterly winds, then switched abruptly to.years of heavy spring
and early summer rains, mild
winters, and frequent Atlantic storms, or to periods of droughts, light northeasterly winds, and summer
heat waves.
C
Reconstructing the climate changes of the past is extremely difficult, because systematic weather observations
began only a few centuries ago, in Europe and North America. Records from India and tropical Africa are even
more recent. For the time before records began, we have only ‘proxy records’ reconstructed
largely from tree
rings and ice cores, supplemented by a few incomplete written accounts. We now have hundreds of tree-ring
records from throughout the northern hemisphere, and many from south of the equator, too, amplified with
a growing body of temperature data from ice cores drilled in Antarctica, Greenland, the Peruvian Andes, and
other locations. We are close to a knowledge of annual summer and winter temperature variations over much
of the northern hemisphere going back 600 years.
D
This book is a narrative history of climatic shifts
during the past ten centuries, and some of the ways in which
people in Europe adapted to them. Part One describes the Medieval Warm Period,roughly 900 to 1200. During
these three centuries, Norse voyagers from Northern Europe explored northern seas, settled Greenland, and
visited North America. It was not a time of uniform warmth, for then, as always since the Great Ice Age, there
were constant shifts in rainfall and temperature. Mean European temperatures were
about the same as today,
perhaps slightly cooler.
E
It is known that the Little Ice Age cooling began in Greenland and the Arctic in about 1200. As the Arctic ice
pack spread southward, Norse voyages to the west were rerouted into the open Atlantic, then ended altogether.
Storminess increased in the North Atlantic and North Sea. Colder, much wetter weather descended on Europe
between 1315 and 1319, when thousands perished in a continent-wide famine. By 1400, the weather had
become decidedly more unpredictable and stormier, with sudden shifts and lower temperatures that culminated
in the cold decades of the late sixteenth century. Fish were a vital commodity in growing towns and cities,
where food supplies were a constant concern. Dried cod and herring were already the staples of the European
fish trade, but changes in water temperatures forced fishing fleets to work further offshore. The Basques,
Dutch, and English developed the first offshore fishing boats adapted to a colder and stormier Atlantic. A
gradual agricultural revolution in northern Europe stemmed from concerns over food
supplies at a time of
rising populations. The revolution involved intensive commercial farming and the growing of animal fodder on
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land not previously used for crops. The increased productivity from farmland made some countries self-
sufficient in grain and livestock and offered effective protection against famine.
F
Global temperatures began to rise slowly after 1850, with the beginning of the Modern Warm Period. There
was a vast migration from Europe by land-hungry farmers and others, to which the famine caused by the Irish
potato blight contributed, to North America, Australia, New Zealand, and southern Africa. Millions
of hectares
of forest and woodland fell before the newcomers’ axes between 1850 and 1890, as intensive European
farming methods expanded across the world. The unprecedented land clearance released vast quantities
of carbon dioxide into the atmosphere, triggering for the first time humanly caused global warming.
Temperatures climbed more rapidly in the twentieth century as the use of fossil fuels proliferated and
greenhouse gas levels continued to soar. The rise has been even steeper since the early 1980s. The Little Ice
Age has given way to a new climatic regime, marked by prolonged and steady warming. At the same time,
extreme weather events like Category 5 hurricanes are becoming more frequent.
